Progress in dendroclimatic studies of mountain pine in northern Thailand

被引:39
作者
DArrigo, R
Barbetti, M
Watanasak, M
Buckley, B
Krusic, P
Boonchirdchoo, S
Sarutanon, S
机构
[1] Tree-Ring Laboratory, Lamont-Doherty Earth Observatory, Palisades
[2] NWG Macintosh Ctr. Quaternary Dating, University of Sydney
[3] Fac. of Environ. and Rsrc. Studies, Mahidol University
[4] Inst. Antarctic and S. Ocean Studs., University of Tasmania, Hobart, Tasmania 7001
关键词
tree rings; dendrochronology; Thailand; mountain pine; monsoon; Southeast Asia; Pinus kesiya; Pinus merkusii;
D O I
10.1163/22941932-90001508
中图分类号
S7 [林业];
学科分类号
0829 ; 0907 ;
摘要
New data added to the existing tree-ring width chronologies of mountain pine (Pinus kesiya and Pinus merkusii) result in a total of seven chronologies for these species for Thailand. The oldest (1647-1993) is from a P. merkusii site at Phu Kradung, north central Thailand. An analysis of the three longest P. kesiya chronologies, from north central Thailand, with Phetchabun rainfall (1951-1992) reveals correspondence between years of low growth and below average rainfall (drought) during the wet season (July-November). The lowest growth year averaged over these three sites during the period of rainfall data (1951-1992) occurred in 1979, coinciding with the lowest wet season rainfall on record. For the common period of tree-ring record prior to 1951 (1830-1950), the level of drought severity in 1979 appears to have been exceeded only twice previously in 1832 and 1894. A P. merkusii record from Thung Salaeng Luang is most significantly correlated with temperatures during May-June, considered a critical period for the subsequent evolution of the Asian monsoon.
引用
收藏
页码:433 / 444
页数:12
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